oc
rdiff 03; ac adine from between centennial to millennial scale fluctuations in the flow speed of Iceland-Scotland Overflow Water inferred from granulometric Holocene climate proxy records indicate the presence of responses that may not be present, at least in the same ARTICLE IN PRESS2. Material and...
Other Authors: | |
---|---|
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.476.1018 http://folk.uib.no/abo007/share/papers/8k/hall_bianchi04.qsr.pdf |
Summary: | rdiff 03; ac adine from between centennial to millennial scale fluctuations in the flow speed of Iceland-Scotland Overflow Water inferred from granulometric Holocene climate proxy records indicate the presence of responses that may not be present, at least in the same ARTICLE IN PRESS2. Material and methods Our climate records have been obtained from kasten core NEAP4K recovered from the rapidly deposited sediments of the Bj.orn Drift, northern Iceland Basin $Table 1 available in the online version of this article, doi:10.1016/ j.quascirev.2004.04.004 |
---|